Here's a reach on why it may happen. Maybe David can tear into this late night idea since it's just speculation on my part.
The extra magnesium could increase the levels of carbonate alk by slowing precipitation(allowing greater saturation) thus leaving a bit more carbonate to take up more H+ for shifts to bicarbonate. In turn less available H+ in the water( higher ph) could shift the PO4,HPO4, H2PO4,H3PO4 to the left perhaps strengthening the bond to calcium carbonate surfaces like live rock reducing any leaching that may be occuring and feeding the bryopsis. The increase in specific gravity from the mag additions might play a role as well.